How it works
A satellite in a circular orbit is in continuous free fall: gravity supplies exactly the centripetal acceleration v²/r needed to bend its straight-line motion into a circle. Setting GMm/r² = mv²/r gives v = √(GM/r).
Because r is measured from the centre of the body, higher orbits are slower. The ISS travels at about 7.66 km/s, while a geostationary satellite moves at only about 3.07 km/s.
Variables
v— circular orbital speedμ— standard gravitational parameter GM of the central bodyr— orbital radius = body radius + altitude
Assumptions and limits
- Circular orbit around a spherical, non-rotating body
- Orbiting mass is negligible compared with the central body
- No atmospheric drag or third-body perturbations
For education only. These models are simplified and are not suitable for spacecraft navigation or safety-critical engineering. See our scientific accuracy policy.